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The data was migrated with source-receiver migration. The depth step was
10 m and 400 depth steps were computed in total. Figure
shows one SODCIG migrated with the correct velocity (left panel) and with
90% of the correct velocity (right panel). Obviously, with the correct
velocity both primaries are well focused around zero subsurface offset,
whereas the multiples are mapped to the negative subsurface offsets. With
the slower velocities, the primaries are now mapped shallower, with
downward moveout and toward the positive subsurface offsets. The multiples
are still mapped to the negative subsurface offsets although they are
somewhat closer to the zero subsurface offsets.
Next: Muting the primary and
Up: Methodology for attenuating the
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Stanford Exploration Project
4/5/2006